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The location of the state of New Mexico. Paleontology in New Mexico refers to paleontological research occurring within or conducted by people from the U.S. state of New Mexico. The fossil record of New Mexico is exceptionally complete and spans almost the entire stratigraphic column. [1] More than 3,300 different kinds of fossil organisms have ...
The river starts in the Sangre de Cristo mountain range and passes through the state capital, Santa Fe providing approximately 40% of the city's water supply. It is an intermittent stream with two perennial reaches. The river is 46 miles (74 km) long. It was first dammed in 1881 and flows when water is released by the city of Santa Fe from two ...
Albuquerque Basin. The Albuquerque Basin (or Middle Rio Grande Basin[1]) is a structural basin and ecoregion within the Rio Grande rift in central New Mexico. It contains the city of Albuquerque. Geologically, the Albuquerque Basin is a half-graben that slopes down towards the east to terminate on the Sandia and Manzano mountains. [2]
Santa Fe, New Mexico. Named by. Hayden. Year defined. 1869. The Santa Fe Group is a group of geologic formations in New Mexico and Colorado. It contains fossils characteristic of the Oligocene through Pleistocene epochs. The group consists of basin -filling sedimentary and volcanic rocks of the Rio Grande rift, and contains important regional ...
Santa Fe (/ ˌ s æ n t ə ˈ f eɪ, ˈ s æ n t ə f eɪ / SAN-tə FAY, - fay; Spanish:) is the capital of the U.S. state of New Mexico, and the county seat of Santa Fe County.With over 89,000 residents, [5] Santa Fe is the fourth-most populous city in the state, [6] and part of the Albuquerque–Santa Fe–Los Alamos combined statistical area, which had a population of 1,162,523 in 2020.
The Ancha Formation is a geologic formation found near Santa Fe, New Mexico. It is estimated to be between 1 and 3 million years in age, corresponding to the late Pliocene and Pleistocene. [1] Study of the formation has provided clues on the development of rivers systems in the region.
The geology of New Mexico includes bedrock exposures of four physiographic provinces, with ages ranging from almost 1800 million years (Ma) to nearly the present day. Here the Great Plains, southern Rocky Mountains, Colorado Plateau, and Basin and Range Provinces meet, giving the state great geologic diversity.
Rio Felix. Rio Hondo (Southern New Mexico) Berrendo River. Rio Bonito. Rio Ruidoso. Arroyo del Macho. Gallo Arroyo. Taiban Creek. Pintada Arroyo.